ライフサイエンスコーパス: Waters

1 nt structural components for life in coastal waters.

2 ease systems for the purification of surface waters.

3 sion of right whale habitat into unprotected waters.

4 nonpoint source of contamination to surface waters.

5 s higher in middle reaches than that at head waters.

6 Thaumarchaeota (4-54%) in temperate Pacific waters.

7 he chemical mixtures present in many surface waters.

8 brought samples more closely similar to tap waters.

9 s aiming at determining nutrients in natural waters.

10 within the upper euphotic zone of temperate waters.

11 antic Oceans, in/over generally oligotrophic waters.

12 ary to maintain chlorine disinfection in the waters.

13 contributions in mesotrophic and open-ocean waters.

14 serpentinite belt and (ii) in local surface waters.

15 lectrodes in the process of treating natural waters.

16 l vorticity (PV) compared to the surrounding waters.

17 apparent" loss of this fraction from surface waters.

18 4 of which had never been detected in marine waters.

19 trophic nutrition in oligotrophic open ocean waters.

20 s, suspended particles, and filtered surface waters.

21 idence of the importance of these vulnerable waters.

22 aromatic amines is shown to occur in surface waters.

23 th no untouched populations known in shallow waters.

24 mproving ecosystem service benefits of urban waters.

25 the nitrification flux in Antarctic coastal waters.

26 of sea turtle density (km(-2)) in nearshore waters.

27 ioavailability of iron in calcium-containing waters.

28 ng a volcanogenic influence on the formation waters.

29 ultispecies meadows in oligotrophic tropical waters.

30 impact of the DITP DSi loading on receiving waters.

31 y as highly reduced species in sulfidic pore waters.

32 ependence as fluctuations of hydration shell waters.

33 ic production occurring in the saline bottom waters.

34 gnificant process occurring in surface ocean waters.

35 ng when birds winter further north in colder waters.

36 of zooplankton particle interactions in OMZ waters.

37 er remain resident or migrate to surrounding waters.

38 therefore to eutrophication of urban surface waters.

39 hich were reported the first time in surface waters.

40 jurisdictional scope for federally protected waters.

41 ting sulfide concentrations in sediment pore waters.

42 genus Synechococcus are ubiquitous in ocean waters.

43 tion in groundwater discharging into surface waters.

44 the presence of Fe(II) in oxic circumneutral waters.

45 rusion or high mineral content in the source waters.

46 ct silver ion release in estuarine or marine waters.

47 ealistic, complex, and heterogeneous flowing waters.

48 n a drawdown of nutrients in oceanic surface waters.

49 r fresh water organisms in recipient surface waters.

50 degradation product in chlorinated drinking waters.

51 rmination of AP, Ph, and NP in tap and river waters.

52 er speciation is poorly defined in estuarine waters.

53 Zn(2+), Y383, E271, D375, and two catalytic waters.

54 e power is challenging for dynamic estuarine waters.

55 gal products in coastal or estuarine surface waters.

56 atellite tags during escapement from coastal waters.

57 dant and widely distributed in nutrient rich waters.

58 ed organic matter (DOM) from land to surface waters.

59 d concentrations of methylated Se in natural waters.

60 otrophic, tropical/subtropical ocean surface waters.

61 genated surface waters and fully anoxic deep waters.

62 ng with heavier isotopic composition in deep waters.

63 scale DCMD treatment of oil and gas produced waters.

64 fully enhance protection of these vulnerable waters.

65 birds killed annually by bycatch in European waters.

66 le metal-based nanomaterials in organic-rich waters.

67 widely distributed in oligotrophic tropical waters.

68 enter nontarget environments, e.g., surface waters.

69 are generally atypical for finished drinking waters.

70 that have been detected in waste and surface waters.

71 ASs) through riverine discharge into coastal waters.

72 notube (MWCNT) fate and transport in surface waters.

73 n (Fe) fertilization of subantarctic surface waters.

74 xposure to concentrations typical of surface waters.

75 xanesulfonate (PFHxS) precursors in Canadian waters.

76 rted by the recycling of iron within surface waters.

77 rage (TWA) measurement of these chemicals in waters.

78 9 +/- 0.04), soils (1.09 +/- 0.02), and pore waters (1.08 +/- 0.02) indicate indistinguishable enviro

79 he most abundant microbes in oceanic surface waters [1-4].

80 As in rice by 23%, the use of different well waters (281-1144mug/L) increased As levels significantly

81 During chlorination of bromide-containing waters, a significant formation of brominated disinfecti

82 high-frequency temperature data from inland waters across the globe confirmed that Tw-Ta is linearly

83 The United States Microbead-Free Waters Act was signed into law in December 2015.

84 can exceed 10 muM during summer in estuarine waters adjacent to Sapelo Island, Georgia, U.S.A.

85 ese probes to DOM isolates and whole natural waters afforded intermediate ratios.

86 lses were observed to disappear from surface waters after low-pressure systems affected the area.

87 antial portion of the organofluorine in some waters and 36-99.7% of the total organofluorine was not

88 cesses such as corrosion of iron in sulfidic waters and abiotic natural attenuation by iron sulfide m

89 ral-West coasts a minor effort, at shallower waters and across a wider range of habitats, is also app

90 n situ SCN(-) biodegradation in mine tailing waters and also yield new insights into the microbial ec

91 mumol m(-2)d(-1)) twice that of surrounding waters and approximately 1,900 times greater than the di

92 strogen mimics are commonly found in surface waters and are associated with deleterious effects in fi

93 (PFOA), contaminate many ground and surface waters and are environmentally persistent.

94 Furthermore, warmer waters and declining zooplankton densities may act toget

95 (DOC) affects both carbon cycling in surface waters and drinking water production.

96 levels of physiological performance in cold waters and facilitates frequent movement across strong t

97 This method was applied to bottled waters and fruit juices purchased in Kaohsiung, Taiwan.

98 quantification of 1ngL(-1) and 5ngkg(-1) in waters and fruits, respectively, while a similar sensiti

99 he 23-119 and 12-60 ranges were obtained for waters and fruits, respectively.

100 narrow zone between well-oxygenated surface waters and fully anoxic deep waters.

101 of acetoclastic production in fresh surface waters and hydrogenotrophic production occurring in the

102 matic stability and connectivity of Japanese waters and its network of marine protected areas (MPAs).

103 for E. verrucosa, a protected species in UK waters and listed by the IUCN as 'Vulnerable', and for t

104 The dramatic mercury loss from deep waters and methylmercury loss from underlying sediment i

105 s part of the normal microbiota of estuarine waters and occurs in high numbers in molluscan shellfish

106 Fe speciation of river waters and salinity-induced aggregates was determined by

107 Accurate pH measurements in polar waters and sea ice brines require pH indicator dyes char

108 In the surface waters and size fractions, peak C was preferentially rem

109 ted pesticides, and five metals in Norwegian waters and Skagerrak.

110 hting the close interactions with structural waters and the local allosteric interactions that couple

111 pore waters exchanges with overlying surface waters and the sulfur likely undergoes oxidative transfo

112 a heat exchange drives the formation of deep waters and the surface circulation of warm waters around

113 s that affects both DOC stability in surface waters and treatability during drinking water production

114 physically demanding, require travel to deep waters, and are considered more sustainable.

115 due to ash input and algal growth in source waters, and consequently impacting disinfection byproduc

116 Analyses of soils, pore waters, and earthworm tissues using multiple collector i

117 r-capita fluxes, loads discharged to surface waters, and economic waste-stream values.

118 centrations in surface waters, sediment pore waters, and resident fish species from coal combustion r

119 Vibrio cholerae, grow in warm, low-salinity waters, and their abundance in the natural environment m

120 been observed in oxygen-rich marine and lake waters, and viewed to significantly contribute to biosph

121 The locations and thermodynamics of the waters are derived from a WaterMap molecular dynamics si

122 Surface ocean waters are dominated by planktonic bacterial lineages wi

123 Inland waters are increasingly recognized as critical sites of

124 Environmental waters are monitored for fecal pollution to protect publ

125 e likely in the near future given that these waters are predicted to shoal from depth over the coming

126 fects of CO2 enrichment on eutrophic coastal waters are still unclear, as are the complex mechanisms

127 lineally maintained autumn migrations in the waters around Alaska and Russia.

128 ps of nitrification by hypoxia; however, the waters around Sapelo Island are aerobic and well-mixed.

129 p waters and the surface circulation of warm waters around the subpolar gyre.

130 lly from those in adjacent limnic and marine waters as well as from cultivated and sequenced picocyan

131 in the plastic industry and found in natural waters at concentrations considered harmful for aquatic

132 of delta(34)S for aqueous sulfide in natural waters at high spatial resolution (<1 mm(2)) with reason

133 in part to their differing interactions with waters at the membrane inner leaf.

134 important oxidants and reactants in surface waters, atmospheric drops, and snowpacks.

135 rsists in eastern equatorial Pacific surface waters because phytoplankton growth fueled by nitrate (n

136 can occur at high concentrations in surface waters but generally has been of lesser concern due to i

137 These were once reliable cues for prey-rich waters, but climate change and industrial fishing have d

138 of fecal indicator bacteria in urban coastal waters, but it is unknown whether exposure to seawater a

139 ion appears to be minor in temperate coastal waters, but may represent a significant portion of the n

140 reducing to oxidizing conditions in natural waters by combining biogeochemical microcosm experiments

141 s from agglomeration in high salinity marine waters by electrosteric repulsion for long time periods.

142 n within an order of magnitude for estuarine waters by using a readily available metal speciation mod

143 re we show that nitrate consumption in these waters cannot be fueled solely by the external supply of

144 or detection Hg(2+) ions from samples of tap waters, carp and saltwater fishes with satisfactory resu

145 aft in the urban Bronx River Estuary, NY, in waters closed to shellfish harvest due to bacterial cont

146 lead to more rapid acidification in coastal waters compared to the open ocean.

147 carbon substrates in the iceberg-influenced waters compared with the undisturbed site.

148 ts of silver nanoparticles (AgNPs) to marine waters continue to increase yet mechanisms of AgNPs toxi

149 forced by increased southward flow of Arctic waters, contributed to modulating the climate of Europe

150 ined whether contaminants present in surface waters could be prioritized for further assessment by li

151 pecies and the resettlement of the oxic deep waters, could lead to the enhanced transfer of accumulat

152 81% and methylmercury concentrations in deep waters decreased by roughly 86% due to destratification.

153 ter Denver area, Minnesota lakes, and Oregon waters, demonstrating a framework for identifying endocr

154 Contamination of surface waters due to run-off, coupled with its moderate solubil

155 deeper layers at night and well-lit surface waters during the day.

156 hat volcanically-induced drainage of Fe-rich waters during the Last Glacial Maximum could have reache

157 f littoral habitat and occupied deep pelagic waters during the summer.

158 be released into soils, ground-, and surface waters either from ore minerals that weather in near sur

159 atural Pb then become entrained into polynya waters either from sediment resuspension or from the tra

160 rmation for protecting and restoring natural waters, enhancing process control for industrial operati

161 t negatively with triplet quantum yields, as waters enriched in highly aromatic formulas exhibit much

162 lysis reveals that the northern-sourced deep waters enter the Antarctic Circumpolar Current via south

163 Sulfur-enriched DOM in sediment pore waters exchanges with overlying surface waters and the s

164 solid-solution equilibria (e.g., in stagnant waters), Fe-rich freshwater flocs are expected to remain

165 ic or national prioritization for monitoring waters for chemicals with endocrine disrupting activity.

166 tor the environmental suitability of coastal waters for Vibrio spp. using remotely sensed SST and sal

167 iofiltration systems to treat other polluted waters, for example greywater, such an understanding is

168 o raise atmospheric pressure to prevent lake waters from being lost to the atmosphere.

169 4 chemicals detected in flowback or produced waters from hydraulically fractured wells.

170 ts conducted with naturally methane-enriched waters from hydrocarbon seeps in the vicinity of the DWH

171 Using this system, we analysed waters from intact and degraded peat swamp forest of Kal

172 agement practices are not protecting surface waters from road salt contamination and suggest they cre

173 ive analysis was used to investigate surface waters from rural, urban, and AFFF-impacted sites in Can

174 , and the resultant contamination of surface waters from the outflow of water treatment facilities is

175 attribute the ECR to upwelling of cold deep waters from the Southern Ocean.

176 oducts (N-DBPs) whose occurrence in drinking waters has recently been reported in several DBP surveys

177 resulting in their presence in environmental waters; however, they have not been widely studied in bi

178 It is frequently detected in surface waters; however, whether this pharmaceutical poses a ris

179 large region of low-dissolved-oxygen bottom waters (hypoxia) forms nearly every summer in the northe

180 cide often inadvertently added to coral-reef waters, impaired visual-lateralization.

181 c-contaminated soil exposed to sea and river waters in biogeochemical microcosm reactors across field

182 rmation during transportation of chlorinated waters in copper-containing distribution systems.

183 and magnesium [Ca + Mg] leaching to surface waters in granitic alpine regions recovering from acidif

184 ent laws to limit CCR discharge into surface waters in NC.

185 the NEP and increased utilization of deeper waters in offshore habitats.

186 haracterized by pronounced formation of deep waters in the NW Atlantic.

187 s, and pharmaceuticals is well documented in waters in the U.S. and globally.

188 arine ecosystems (LMEs) covering all coastal waters in the world.

189 idiosyncratically at high levels in some tap waters, indicating distribution and/or premise plumbing

190 Natural waters interacting with bauxite residue are characterist

191 Seepage of SCN(-)-contaminated waters into aquifers can occur from unlined or structura

192 atial mosaic in the penetration of acidified waters into ecologically-important nearshore habitats ac

193 CO2 and CH4 transfer velocities from inland waters into the atmosphere.

194 showing the incursion of deep Southern Ocean waters into the tropics and subtropics.

195 Primary production in sunlit surface waters is channelled through complex food webs that exte

196 speaking, N-Cl-HAMs in chlorinated drinking waters is of significance because they are organic chlor

197 redox reactions to acidification in coastal waters is unclear.

198 ildlife overharvesting in forests and inland waters is unknown.

199 2, His-143, Thr-139, His-189, and structural waters, is located at the edge of PLP opposite the react

200 ams, Cr(VI) levels measured in local surface waters largely remain below California's drinking water

201 Oxygen consumption in its deep waters leads to the buildup of sulfide from sulfate redu

202 d from underwater visual censuses in shallow waters (</=30 m).

203 Si-limitation is reflected in the receiving waters (Massachusetts Bay).

204 of organisms, biota in estuarine and coastal waters may be particularly vulnerable.

205 is indicated that DCMD treatment of produced waters may require additional processing to meet dischar

206 ased climate variability and warming coastal waters may therefore increase the frequency of these nit

207 hat coastal seaweed assemblages in eutrophic waters may undergo an initial shift toward communities d

208 atively small safety margin for some surface waters may warrant a longer term chronic health effects

209 This suggests that nitrite peaks in coastal waters might be explained by differences in the response

210 e produced via hydrogen sulfide oxidation in waters mixed upward from anoxic depths.

211 re generated as a result of H2S oxidation in waters mixed upward from the anoxic depths.

212 r samples were collected from 3 urban source waters (municipal tap water, streamwater, and wastewater

213 ld greater flux of particulate Pb to abyssal waters near the Asian continent.

214 that ventilation of EEP thermocline and deep waters occurred synchronously during the last deglaciati

215 ar, Mycobacterium spp., very low in finished waters, occurred idiosyncratically at high levels in som

216 s (AZAs) are being reported from the coastal waters of an increasing number of countries on a global

217 te for in-situ incubation studies in shallow waters of Catalina Island, CA to investigate the coloniz

218 hians, deliberately crawls into the alkaline waters of Mono Lake to feed and lay eggs.

219 The sediment pore waters of PPR wetlands contain some of the highest conce

220 es S to the mixed layer is 60-90 years.Deep waters of the Atlantic, Pacific and Indian Oceans upwell

221 ea temporally re-establish oxic life in deep waters of the Baltic Sea.

222 n Francisco Bay with those in adjacent shelf waters of the California Current System (CCS) that are s

223 trations and (236)U/(238)U ratios in surface waters of the North Sea can be explained by simple binar

224 ibian Proteus anguinus inhabits subterranean waters of the north-western Balkan Peninsula.

225 on their localization within the stratified waters of the SBB we hypothesize a dynamic and annular b

226 Total mercury concentrations in the deep waters of the south arm decreased by approximately 81% a

227 ion rates (OUR) reported for the mesopelagic waters of the subtropical North Atlantic.

228 of three migration behaviours: remaining in waters of UK, Ireland and the Faroe Islands; migrating s

229 ntic Ocean, with a decrease in detections in waters off Cape Hatteras, North Carolina in summer and f

230 the Bay of Biscay or moving further south to waters off the Iberian Peninsula, and North Africa.

231 zon was the largest marine oil spill in U.S. waters, oiling large expanses of coastal wetland shoreli

232 he air to survive warm, oxygen-poor stagnant waters or overland excursion under moist condition.

233 ordeum vulgare was investigated in different waters or soils, totaling 30 different experiments.

234 Once in complex media such as environmental waters or toxicology exposure media, the same redox tran

235 In sunlit waters, photochemical alteration of dissolved organic ca

236 y greater aggregation occurred in mesohaline waters (possibly due to higher salinity), which may have

237 es in DOM and consequent browning of surface waters reduce the potential for solar UV inactivation of

238 To alleviate eutrophication in coastal waters, reducing nitrogen (N) discharge from wastewater

239 xpectedly low DOC concentrations in the pore waters, reflecting the combined effect of thermal desorp

240 position were observed in iceberg-influenced waters relative to the undisturbed water column nearby.

241 These high-salinity waters require the use of thermally driven treatment pro

242 oving nutrients from the deep sea to surface waters, seabirds and anadromous fish moving nutrients fr

243 measured selenium concentrations in surface waters, sediment pore waters, and resident fish species

244 centration is to be expected, even in acidic waters, since time scales of light-mediated Fe(III) redu

245 ltiple metals are usually present in surface waters, sometimes leading to toxicity that currently is

246 g a SYNAPT High-Definition MS (HDMS) System (Waters) specifically for metabolomics and lipidomics app

247 nd amorphous particulate silica into natural waters stimulates the growth of diatoms.

248 e expected kinetic fractionation of meteoric waters, suggesting a volcanogenic influence on the forma

249 revalence in expanding, low nutrient surface waters suggests they will have a role in future oceans.

250 the lateral boundary conditions and coastal waters surrounding the continental U.S. is examined usin

251 ith detection using a commercial instrument (Waters Synapt G2).

252 ing the separation of the different types of waters that are released at different temperatures.

253 l biogenic and geogenic materials in natural waters that interact with and modify the surface of ENMs

254 distributions observed globally within open waters that remains unexplained.

255 optimization modeling we highlight lands and waters that together achieve joint conservation goals fr

256 ar fluids, allowing fish to function in cold waters that would otherwise freeze them.

257 In anaerobic bottom waters, the natural tracer radon ((222)Rn) revealed that

258 benzotriazoles (BTs) are ubiquitous in urban waters, their sources and transport remain poorly charac

259 an enhance CO2 and CH4 emissions from inland waters, thereby contributing to increased greenhouse gas

260 tunities for DOC oxidation to CO2 in surface waters, thereby reinforcing global warming.

261 grating further and visiting less-productive waters; this in turn led to differences in flight activi

262 in samples from Antarctic continental shelf waters, though the difference was not statistically sign

263 d organic matter (DOM) to inland and coastal waters through increases in precipitation, thawing of pe

264 timates of the other C fluxes through inland waters to derive a C budget for the boreal region, and f

265 the transport of sediment-laden glacial melt waters to the polynya.

266 Upwelling of global deep waters to the sea surface in the Southern Ocean closes t

267 We find 88% of Japanese waters transitioning to climates outside their historica

268 Arsenic occurs in marine waters, typically at concentrations of 1-2 mug As kg(-1)

269 tions mediated by SRFA in calcium-containing waters under irradiated and nonirradiated conditions.

270 k has implications for the photochemistry of waters undergoing natural or engineered treatment proces

271 deeper distribution makes their exposure to waters undersaturated for aragonite more likely in the n

272 nental shelf, and include ocean systems with waters up to 50 meters in depth.

273 r instrument-free determination of cobalt in waters using distance-based readout, with excellent prec

274 onfirm proton transport occurs through these waters via Grotthuss shuttling and reveal that proton bi

275 n in glacial runoff and near surface coastal waters was aged (12100-1500 years BP (14) C-age) but dis

276 DOM from surface waters, wastewater effluent, and 1 kDa size fractions we

277 ting the molybdate reactive P (MRP) in these waters were analyzed using the data of the past decade (

278 Iron-speciation indicates deeper waters were anoxic and Fe-rich, while trace element conc

279 race element concentrations indicate surface waters were in contact with an oxygenated atmosphere.

280 hiISC for different DOM isolates and natural waters were quantified; values ranged from 12 to 26 mus

281 solved inorganic carbon and biota in coastal waters were young (530 years BP (14) C-age to modern).

282 fresh leaf leachate and two humic-rich lake waters, were analyzed by the direct method presented her

283 sharks generally reduced their use of deeper waters when encountering the combination of cold tempera

284 ng platforms enable self-calibration in deep waters where pH values are stable.

285 or other transformation processes in natural waters where radical intermediates are generated.

286 uences of the oxygenation of Baltic Sea deep waters, which are the coprecipitation of mercury species

287 re able to outcompete diatoms in Si-depleted waters, which can contribute to the formation of coccoli

288 ce of phosphorus-bearing, N-depleted surface waters, which encourages N2 fixation, the dominant N inp

289 lely by the external supply of iron to these waters, which occurs by upwelling and dust deposition.

290 rations and hence Fe availability in natural waters will significantly increase in the presence of th

291 remove 70% soluble phosphorus from eutrophic waters with 0.35 g m(-3) soluble phosphorus would includ

292 tagenicity has been observed in many surface waters with a possible link to the presence of aromatic

293 es of primary producers to OA, especially in waters with diatom-dominated phytoplankton assemblages.

294 ng applications for wetland, river, and lake waters with high terrestrial dissolved organic matter in

295 spp. are pathogenic and ubiquitous in marine waters with low to moderate salinity and thrive with ele

296 e resulting in-line acidification of natural waters with millimolar sodium chloride level (freshwater

297 ould be at least partly due to sampling over waters with much lower biological activity than in previ

298 rsistence in living systems and oxic natural waters, with important implications for biomedical appli

299 ation of hydrocarbons from frac and produced waters without fouling.

300 tanding of carbon cycling in macroalgae-rich waters worldwide.

301 nd if more broadly distributed across inland waters would play an important role in continental N-cyc